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Community Characteristics of Dominant Archaea before and after the Danjiangkou Dam
LIN Yaxuan, DANG Chenyuan, ZHONG Sining, WANG Jiawen, ZHENG Tong, NI Jinren
Acta Scientiarum Naturalium Universitatis Pekinensis    2020, 56 (3): 509-517.   DOI: 10.13209/j.0479-8023.2020.034
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The 16S rRNA Illumina Miseq high-throughput sequencing technology was used to analyze the species composition of archaea in the Danjiangkou reservoir area and the downstream Hanjiang River. The structure of ammonia-oxidizing archaea (AOA) and methanogenic archaea that dominated the water and sediments in the upstream and downstream dam was analyzed. The results showed that the structure of the dominant species was affected by the samples difference, which could be explained by the aerobic preference of the ammonia-oxidizing archaea and the anaerobic properties of the methanogenic archaea. According to the network analysis, there was a significant correlation between the ammonia-oxidizing archaea and the methanogenic archaea in the upstream of the Danjiangkou reservoir. Because of the operation of the Danjiangkou reservoir, the abundance of ammoniaoxidizing archaea in the water and sediments of downstream of the dam was reduced, and the abundance of methanogenic archaea in the sediments was relatively high. The relation between them was not obvious.
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Redox Variation during the Early and Middle Ordovician in South China and Its Implication to the Great Ordovician Biodiversification Event
DONG Yiting, LIU Jianbo, CHEN Yuxuan, ZHONG Si, ZHAN Renbin
Acta Scientiarum Naturalium Universitatis Pekinensis    2018, 54 (4): 739-751.   DOI: 10.13209/j.0479-8023.2017.133
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To improve understanding of the environmental influential and controlling factors of the Great Ordovician Biodiversification Event (GOBE), total organic carbon content (TOC), total sulfur content (TS), and sulfur isotope of pyrite (δ34Spy) of black shale of the Jiangjunling section, in southern Anhui Province, China are analyzed. TOC and TS show positive correlation, indicating non-euxinic environment. δ34Spy exhibits obvious decrease in Floian and more oscillation in the Middle Ordovician. Combined with global sulfur isotope of carbonate-associated sulfate (δ34SCAS) and δ34Spy data from previous researches, a marine oxygenation event is suggested by decreasing pyrite burial and increasing sulfur isotopic fractionation during the latest Tremadocian to middle Floian, which might boost GOBE. During the late Floian to Darriwilian, δ34SCAS from different areas decreases in succession, while δ34Spy is characterized by large oscillation, which is contributed to low sulfate concentration and sulfide reoxidation in the ocean.

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